Presentation on theme: "A trip through geologic time Chapter 10 page 310"— Presentation transcript:
1 A trip through geologic time Chapter 10 page 310 March 2012By award winning Mr. Huppert
2 Fossils Section 1 page 310 1. What is a fossil? A fossil is the preserved remains or traces of living thingsProvides evidence of how life changed over timeProvides clues to what past environments were like
3 Fossils 2. How does a fossil form? An organism dies. Sediment covers the remains. The sediment becomes rock.2 a. What type of rock do fossils form in?Sedimentary
5 Fossils continued Mold fossils 3. What is a mold fossil and how does it form?A hollow area in sediment in the shape of an organism. Forms when the hard part of the organism is buried in sediment.
6 Fossils continued Cast fossils 4. What is a cast fossil and how does it form?A cast fossil is a solid copy of the shape of an organism. A cast is the opposite of a mold.
7 Fossils Petrified 5. What is a petrified fossil? A fossil in which minerals have replaced all or part of the organism.
8 Fossils Carbon film 6. What are carbon films? An extremely thin coating of carbon on rock from the organism.
9 Fossils continued 7. Describe trace fossils: Trace fossils can tell us about the organisms size, behavior, number of feet, whether or not it traveled in groups, etc…
10 Fossils 8.What are some other ways organisms can be preserved? Organisms can be preserved in tar, amber, and ice.
11 Almost done with fossils! 9. What is the name of the type of scientist that studies fossils?A Paleontologist
12 Fossil Record 10. What is the fossil record? The fossil record provides evidence about the history of life and past environments on Earth. It shows how different groups of organisms have changed over time.
14 Done with fossils!11. What is the name of the theory that describes and explains the change of organisms over time?Evolution
15 The relative age of rocks Section 2 pg. 317 1. What is the difference between relative and absolute age?Relative age is the age of a rock compared to the ages of other rocks. Absolute is the exact (within a few years) age of the rock.
16 Superposition 2. What is the law of superposition? The oldest rock layers are on the bottom. Each higher layer above is younger.
17 The relative age of rocks continued 3. How do scientists determine the relative age of rocks?They look at extrusions, intrusions, faults and gaps in the geologic record.Extrusions are always younger than the rocks below itAn intrusion is always younger then the rock layer around or beneath it.
18 Relative age4. How can scientists use fossils to date rocks and what is an index fossil?Fossils that are widely distributed and represent an organism that lived only briefly can tell the relative ages of the rock layer they are in. The fossils are called index fossils.
20 Radioactive Dating Section 3 page 323 Describe in detail radioactive decay:Radioactive decay occurs when certain elements breakdown or decay into a different version of the same element or into a new element. The rate of decay is constant (called half life). Half life is the amount of time it takes half of the atoms to decay over time.
21 Radioactive Dating continued 2. Does radioactive dating determine absolute or relative age?Absolute3. What are the two most common radioactive elements used in radioactive dating?Potassium- argon and Carbon 14
22 The Geologic Time Scale Section 4 page 327 1.What is the geologic time scale?A record of life forms and geologic events in Earth’s history.2.What criteria did scientists use to determine how to divide up the units of geologic time?They used major changes in life forms at certain times.Era- one of the three long units of time between Precambrian and presentPeriod- the unit that is used to divide era’s
23 The Early Earth Section 5 page 330 1. How long ago do scientists believe the earth formed?4.6 billion years ago2. How do scientists know this?Through radioactive dating of rocks
24 Early Earth 3.How did the earth take shape? (how did it form?) It began as a ball of dust and rock pulled together by gravity. Denser material sank to the core. The collisions made the planet very hot.
26 Early Earth 4. How many atmospheres do we think the earth had? Two 5.What happened to the first atmosphere?It was destroyed by the sun- solar storms. (Our mortal enemy)6.How do we believe the oceans formed?Water vapor in the atmosphere condensed and accumulated forming the oceans.
27 The Early Earth continued 7. Describe the first life on earth:Single celled similar to todays bacteria. (Very simple)